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41.
《国际水土保持研究(英文)》2021,9(4):605-619
Headwater streams play a major role for provision of ecosystem services, e.g. drinking water. We investigated a high-altitude headwater catchment of the Kharaa River (including 41 1st-order rivers) to understand the impact of land cover (especially forest cover), environment and human usage on runoff, chemical water quality and macroinvertebrate fauna in a river basin under discontinuous permafrost conditions in an arid, sparsely populated region of Mongolia. To verify our hypotheses that different landuses and environmental impacts in permafrost headwaters influence water quality, we investigated 105 sampling sites, 37 of them at intermittent stream sections without water flow. Discharge was positively impacted by land cover types steppe, grassland and forest and negatively by shrubland, forest burnt by wild fires (indicating a reduction of permafrost) and slope. Water quality was affected by altitude, longitude and latitude, shrub growth and water temperature. Shannon diversity of macroinvertebrates was driven by water temperature, iron content of the water, flow velocity, and subbasin size (adjusted R2 = 0.54). Sample plots clustered in three groups that differed in water chemistry, macroinvertebrate diversity, species composition and bio-indicators. Our study confirms that steppes and grasslands have a higher contribution to runoff than forests, forest cover has a positive impact on water quality, and diversity of macroinvertebrates is higher in sites with less nutrients and pollutants. The excellent ecological status of the upper reaches of the Kharaa is severely threatened by forest fires and human-induced climate change and urgently needs to be conserved. 相似文献
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- Few reports exist that describe marine non‐native species in the Southern Ocean and near‐shore waters around the Antarctic continent. Nevertheless, Antarctica's isolated marine communities, which show high levels of endemism, may be vulnerable to invasion by anthropogenically introduced species from outside Antarctica via vessel hull biofouling.
- Hull surveys of the British Antarctic Survey's RRS James Clark Ross were undertaken between 2007 and 2014 at Rothera Research Station on the Antarctic Peninsula (Lat. 67°34'S; Long. 68°07'W) to investigate levels of biofouling. In each case, following transit through scouring sea‐ice, over 99% of the vessel hull was free of macroscopic fouling communities. However, in some surveys microbial/algal biofilms, balanomorph barnacles and live individuals of the cosmopolitan pelagic barnacle, Conchoderma auritum were found in the vicinity of intake ports, demonstrating the potential for non‐native species to be transported to Antarctica on vessel hulls.
- Increasing ship traffic volumes and declining duration of sea ice in waters to the north and west of the Antarctic Peninsula mean the region may be at increased risk of non‐native species introductions. Locations at particular risk may include the waters around popular visitor sites, such as Goudier Island, Neko Harbour, Whalers Bay, Cuverville Island and Half Moon Island, and around northern peninsula research stations.
- Simple and cost‐effective mitigation measures, such as intentionally moving transiting ships briefly through available offshore sea ice to scour off accessible biofouling communities, may substantially reduce hull‐borne propagule pressure to the region. Better quantification of the risk of marine non‐native species introductions posed by vessel hulls to both Arctic and Antarctic environments, as sea ice patterns and shipping traffic volumes change, will inform the development of appropriate regional and international management responses.
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Soil protection for a sustainable future: options for a soil monitoring network for Ireland 下载免费PDF全文
The increased recognition of the importance of soil is reflected in the UN Post‐2015 Development Agenda with sustainable development goals that directly and indirectly relate to soil quality and protection. Despite a lack of legally binding legislation for soil protection, the European Commission remains committed to the objective of soil protection. However, the achievement of a legally binding framework for soil protection relies on the implementation of a soil monitoring network (SMN) that can detect changes to soil quality over time. As beneficiaries do not pay for the provision of soil information, the options for soil monitoring are limited. The use of existing data sets should be considered first. Using Ireland as an example, this research explored the opportunities for a SMN for Ireland considering three existing national data sets. The options for a SMN are considered in terms of their spatial and stratified distribution, the parameters to be measured and an economic analysis of the options proposed. This research finds that for Ireland, either a 10 or a 16 km2 grid interval stratified by land use and drainage class offers the best potential in relation to the spatial distribution of existing data sets to reflect local data at a national level. With existing data, the stratified SIS data using the 16 km2 grid offers the best value for money, with baseline costs for analysis, excluding field costs, of between €706 481 and €2.8 million. Acknowledging the impossibility of measuring all parameters with ideal frequency, this study proposes a two‐tier system for optimized monitoring frequency. Parameters must anticipate future policy requirements. Finally, the implementation of a SMN must be accompanied by standardized methods, defined thresholds and action mandates to maintain soil quality within allowable limits. 相似文献
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本研究利用CASA(Carnegie-Ames-Stanford Approach)模型模拟了2000—2013年青藏高原草地净植被生产力(Net Primary Production,NPP),结合实测数据、气象数据和土地覆被数据计算了草地降水利用效率(PUE),探究其时空分布特征,以及不同草地类型PUE及其对气候变化的响应。结果表明:青藏高原草地PUE在研究年限内呈现波动增加趋势,增加速率为每年0.0035 g·m-2·mm-1,14 a的平均值为0.38 g·m-2·mm-1。PUE的空间分布具有明显的异质性,呈现东部高、中西部低的基本格局。PUE分布在0.2~0.4 g·m-2·mm-1之间的比例最大,占青藏高原总面积的55.63%,呈减少趋势的区域主要分布在青藏高原的北部和西部,以及东部的边界地区,呈增加趋势的地区集中在研究区的中部和南部。研究年限内PUE的变异系数分布在0.07~0.85之间,变化稳定的区域所占面积最大,为总面积的43.43%,主要分布在唐古拉山脉和横断山脉附近。不同草地类型间PUE均值存在差异,具体表现为:草甸(1.06 g·m-2·mm-1)>坡面草地(0.80 g·m-2·mm-1)>平原草地(0.30 g·m-2·mm-1)>高山与亚高山草甸(0.29 g·m-2·mm-1)>荒漠草地(0.23 g·m-2·mm-1)>高山与亚高山草地(0.094 g·m-2·mm-1)。总体上,青藏高原草地PUE与降水成负相关关系,而与气温呈正相关,PUE的变化对降水响应更加敏感。 相似文献
48.
安全、合理使用农药是农业生产的重要环节,也对农业生态环境和农民的身体健康有着重要影响。通过对六安市金安区农药安全使用的调查,总结了普遍存在的问题。今后植保部门应加强示范、宣传、指导、培训工作,同时大力推广农作物病虫害专业化防治模式,保障农业健康发展,保护农村生态环境。 相似文献
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基于Google Earth Engine平台的关中冬小麦面积时空变化监测 总被引:1,自引:0,他引:1
以关中地区为研究区,基于Google Earth Engine(GEE)平台,根据冬小麦生育期内归一化植被指数(NDVI)时序曲线和物候特征,采用NDVI重构增幅算法和光谱突变斜率,构建了关中地区冬小麦提取模型并实现了冬小麦种植面积的提取。用农业统计面积验证提取结果表明:在市级和县级尺度上,决定系数R~2分别为0.82和0.62,一致性指标d分别为0.95和0.84,提取结果与实地调查数据的空间一致性精度为93.4%。结果显示:关中地区冬小麦主要分布在中部关中平原,冬小麦种植面积在2011—2017年呈下降趋势,减少了83.22×10~3 hm~2(8.47%)。综合考虑冬小麦NDVI时序曲线的"峰""谷"特征,具有一定的普适性,可为大面积连续年份冬小麦种植面积时空监测提供参考。 相似文献
50.
长武塬区苹果园和农田相互转换的深层土壤水环境效应 总被引:1,自引:0,他引:1
研究长武塬区苹果园和农田相互转换后0~1 000 cm土壤含水量特征,分析了苹果园土壤干燥化和苹果园转换为农田后土壤水分的恢复效应。结果表明:2、7、17、23、29 a苹果园200~1 000 cm的平均土壤含水量分别为22.8%、21.4%、16.8%、15.4%、14.9%。500~1 000 cm土层中,29 a苹果园平均土壤含水量(14.5%)高于23 a的果园(13.3%);17~29 a的苹果园均表现为轻度干燥化;基于苹果园和农田转换后土壤水分变化情况估算,苹果园最大种植年限为21 a。苹果园转换为农田1、5、10 a后,农田200~1 000 cm土层土壤含水量分别为:15.3%、15.7%和16.2%,恢复到土壤稳定湿度以上的土层厚度分别为140 cm(1 a)、220 cm(5 a)和400 cm(10 a)。 相似文献